CMS-Flow:Hydro Eqs: Difference between revisions

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         <math> \frac{\partial h  }{\partial t} + \frac{\partial (h U_j )}{\partial x_j} = S </math>
         <math> \frac{\partial h  }{\partial t} + \frac{\partial (h U_j )}{\partial x_j} = S </math>


{{NumBlk|:|<math> \frac{\partial h  }{\partial t}
{{NumBlk|::|<math> \frac{\partial h  }{\partial t}
+ \frac{\partial (h U_j )}{\partial x_j} = S </math>|{{EquationRef|1}}}}
+ \frac{\partial (h U_j )}{\partial x_j} = S </math>|{{EquationRef|1}}}}



Revision as of 20:52, 18 May 2010

Governing Equation

The depth-averaged 2-D continuity and momentum equations are given by

        ht+(hUj)xj=S

Template:NumBlk

for j=1,2

        (hUi)t+(hUiUj)xjϵij3fcUjh=ghηxjhρ0paxj+xj(νthUixj)+τiρ  

for i=1,2 and j=1,2

Symbol Description Units
t Time sec
h Total water depth h=ζ+η m
ζ Still water depth m
η Water surface elevation with respect to the still water elevation m
Uj Current velocity in the jth direction m/sec
S Sum of Precipitation and evaporation per unit area m/sec
g Gravitational constant m/sec2
ρ Water density kg/m3
pa Atmospheric pressure Pa
νt Turbulent eddy viscosity m2/sec

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